Передаточная функция динамической системы атмосфера-океан в диапазоне градиентно-вихревых волн.

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Передаточная функция динамической системы атмосфера-океан в диапазоне градиентно-вихревых волн. / Belonenko, T. V.; Fux, V. R.

в: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, № 2, 1998, стр. 97-101.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

BibTeX

@article{a50906898fef48b482146d30e2bb081d,

title = "Передаточная функция динамической системы атмосфера-океан в диапазоне градиентно-вихревых волн.",

abstract = "In the framework of the linear barotropic hydrodynamical model an expression is derived for the transfer function of the dynamical atmosphere-ocean system within the synoptical frequency range. As input processes the air pressure and the shear stress of the wind were considered, and the sea level was the output. Numerical experiments were made relating to the elementary modes of the gradient-vortex waves: Rossby waves, current waves and topographical waves. The resonance wavelengths were determined at the periods of 3, 10 and 30 days, and the resonance areas were located.",

author = "Belonenko, {T. V.} and Fux, {V. R.}",

year = "1998",

language = "русский",

pages = "97--101",

journal = "Вестник Санкт-Петербургского университета. Науки о Земле",

issn = "2541-9668",

publisher = "Издательство Санкт-Петербургского университета",

number = "2",

}

RIS

TY - JOUR

T1 - Передаточная функция динамической системы атмосфера-океан в диапазоне градиентно-вихревых волн.

AU - Belonenko, T. V.

AU - Fux, V. R.

PY - 1998

Y1 - 1998

N2 - In the framework of the linear barotropic hydrodynamical model an expression is derived for the transfer function of the dynamical atmosphere-ocean system within the synoptical frequency range. As input processes the air pressure and the shear stress of the wind were considered, and the sea level was the output. Numerical experiments were made relating to the elementary modes of the gradient-vortex waves: Rossby waves, current waves and topographical waves. The resonance wavelengths were determined at the periods of 3, 10 and 30 days, and the resonance areas were located.

AB - In the framework of the linear barotropic hydrodynamical model an expression is derived for the transfer function of the dynamical atmosphere-ocean system within the synoptical frequency range. As input processes the air pressure and the shear stress of the wind were considered, and the sea level was the output. Numerical experiments were made relating to the elementary modes of the gradient-vortex waves: Rossby waves, current waves and topographical waves. The resonance wavelengths were determined at the periods of 3, 10 and 30 days, and the resonance areas were located.

UR - http://www.scopus.com/inward/record.url?scp=0032454628&partnerID=8YFLogxK

M3 - статья

SP - 97

EP - 101

JO - Вестник Санкт-Петербургского университета. Науки о Земле

JF - Вестник Санкт-Петербургского университета. Науки о Земле

SN - 2541-9668

IS - 2

ER -

ID: 5016850